STRUCTUlULllDDlSBRHODYl?~C FmuLIAR1!cIBs0P~BOmDARP LUERSOFLIQUIXS B.V.Derjagu3.n Institute of Physical Chemistry of the Academy of Sclenoea 0f the mm, 31, ma13kii Pr08pect, ~00~0~ 117312, u s s R
Gibbs' theory
of oapillaritj,whose centenary anniVer8ary
of publicati-
on haa recently been celebratedat the Leningrad Sympoeium, contemplate6the eurfaoe sone8 at the interface as pos8eaeingproperties that are different from those of phaeee in bulk.In that case, however, a question is left to be anauered as;50 how the properties
Inaide those !#oneB are distributedand
what 58 their tbiakneee.!Chue,Gibbs followers had to solve the problem of providing the specific contenta for the general
thermodmamic
At first, the peculiaritieeand effects have been considered,that are not attributableto the changes in the etrwtuce of liquid (or solvent) as caused by the interface. In the firat place, these comprise the effects depending on the surface field8 of the Van der Waale origin and their overlapping (Lifahite'theory), and the effect8 depending on diffuse ionic atmospheresand their overlapping. It would be advisable to interprete those effects quantitativelyfor the Case of plane-parallelinterlayersa8 two componentsof disjoining presmre. In the case of lyophobic syeteme, it is the taking into account of those Go componentsthat allowed the consecutive theory of stability of lyophobic oolleide to be develeped 1 . Iu epite of the faot that this theory hae been developi.ng already during 42 year6, there remains much to be supplemented. One of the main questions consists in finding correct boundary conditionc~ in integrating Poi#aon-Boltsmonngsequation. It is umaally aesumed that the potential is constant at i&e boundaries of a diffuse ionic layer. This condition ie acceptable 80 far ae the interlayer thickneee is of the order of ionic atmoophereeor thicker. It ie just this thicknees that correspond8to the feroe or potential barrier lf the interactionof partlolee.So, this 355
9. V. Derjaguin juetifies
using
the
asmlnption of the potential constancy in the theory of
stability of lyophobic colloids and in calculating the far potential pit. The eituation,
however, chaqes
for the opposite case of au interlayer that
is much thinner thau the Debyelength.
This we have to deal with in the case
of secondary black free or emulsion film,
or at such aggregation state of
colloidal particles, when the liquid interlayer between them remain8 even after the overcoming of the petential barrier. Certain autho8 2 explain its existence and the peaeibility of it8 subsequent peptization in the following uauuer: at a rapid approach of particles to one another, the adsorption equilibrium ha8 net time to chauge, ewiug to which the last step of approach OCCuPs at COnStaut Charge8 Of SurfaCeS. It is their rather slow relaxation that is able to explain the inpO88ibiliQ
of peptisation after the lengthy
aggregation state. This explanation, however, i8 inapplicable to the etability
of secondary black filus, which 8OBleti1148 psrSiSt8 for year6 and ariSe
al8o at the
slew thW;out
of primaryfilm8.Another
is possible, which should be suitable for interpreting
appreach,however, the stability of any
ultrathin interlayers. In this approach, the mechanior Of charging Surfaces is used as the basis, which allows the surface charge to be calculated in a substantiated way as a function of the interlayer thiclmess. We limit ourselves to the simple case of a diluted 8OlutiOn Containing only one ion-active tenSide, as for example, auion-active eodium oleate. In the aa8e of a sufficiently small thickness of the 8olution interlsyer,which i6 much 8maller than that of the ionic atmesphere, its content of free anions may be neglected. All the auions will be found in adserbed monolayers at the interlayer surfaoes owing te specific adsorption. Part of anions will be blacked by cations, and only the remainingpartof unit area, G
the first determines
the charge of the surface6 per
.
In view of the condition of eleotriaal neutrality, this charge ie compensated for by the charge of cation8 that are present in the film volmt ,,J&dx, where
C(x) is
-h the concentration of oations at a distance of X
symmetry plsne of the film, /t is itu half=thiGkWSS thickness of an ads&tion
(1) from the
(en subtracting the
nonelayer). The adeorption i8etherm will be de-
termined by writing the condition of detailed equilibrium between the proces8es of adrrorption and dosorption
of oatienm
357
SelectedWorkse-c,
=
k (G-CT) ,
(2)
where c,is the concentrationof cations directly close to adsorptionmonolayers; 6,is the charge of surfaces when the adsorbed cations are absent, 80 that difference (Cc- G)is proportionalte the number of the cations adsorbed; & Is the equilibriumconstant. The left side of Equation (2) Is proportionaltc the adsorptionrate, because e
Is proportionalte the num-
ber of "vacant places", which is determinableby the number of anions that are "not blocked" by cations. Instead of Equation (2). we nay writer
Poisson-Boltamam'8 Bquation givest
x2=-Tec,y
(4)
where It,is the potential, E IS the permittivitj;@= Boltzmann constant,T
is the Kelvin temperature, C,
kT
where
k ia the
is the concentration
of cations in the bulk phase, with which the Interlayeris In contact or In the full thermodynamic
equilibrium (in the case of an isolated film).Using
Boltzmaunlsequation,
It will be possible to convert the integral of Equation (4) to:
2% Es
$
= c,-
(6)
c,=
WheN,
(7) designates some length which may be much smaller than d , i.e. the thickness of ionic atmspheres in the solution bulk, if c,- the concentrationof CatiOna
in the eyrmetry
plane of the film
is much higher thsn &., : thie
is realieed at sufficientlysmall values of h_ . For further simplification,we shall examine limit cases of fmall and great thickne8se6.Vhen
,
L< then+
1
(8)
naj be replaced by its argument, snd after carrying out rather s simple calculations,we find:
8. V. Derjaguin
358
As the interlaJerthickness h decreases, the values of CO and
C, > c,
Increase.Let us first consider the case, when c, and CO still remain much smaller thsn g\ , which has a great value. In this case, we obtain from Zquation (3):
In such a case, we derive from Equation (9)t
26,
c
*=zz
(10) l
As Is knem, according to Langmulr 3 , the electrostaticcomponent of disjoining pressure, /7= , is equal to:
(11) Hence, taking into account that for suf+flciently smell values of k
co,> c,,
(12) (13)
ma
is jet not a limit law. At still smaller values of h. , the concentra-
tion of C, will be inoreased to such an extent that the Inverse condition will be reallsedt
c, >> g and similtaueouslj c,*
c,.
(14)
Then from Equations (3) and (9). we deriver
(15)
(16) (17)
We shall have enother limit case, when the taugent argument in formula (6) vi11 tend to 9
, cud when accordiugl~ C,L;< C,. Supposing,however,
that Oondltion C,>>c,is I,=&& Consequently:
preserved,we obtains
359
SelectedWorks- 1
Xormula (21)
coincides
with Langnuir*s
formula
that has been
the case where k is substantially
smsller thau the thicknsss
mospheres, while the dimensionless
potential
than unitJ, which coincides
with conditions
of Equation (12) consists
culiaritJ meters G,
of Sonic at-
of surfaces
is much greater
(18) snd (19).
An essential
in that 0,
depends on adsorption
pepara-
and & . Go , its
As regards
range. It will
value is within a narrow range, when the monolay-
be the higher,
and ths cations
The value of & msy vary within a wide
to saturation.
er is dense and close
respect,
derived for
the easier
the adsorbed molecules dissociate
pass over from the monolayer into ths film bulk. In this
lithium and sodium ions occupy the first
ens, both kinds of ions exhibiting
an increased
, the following
place in aqueous aolutihydration energy. On having
assessed possible
values of
&
csn be established
ple calculations:
transition
with a deorease in /L from formula (21) to
formulas (13) and (17) Is accompanied by a drastic magnitude) Increase
In n,
in fle with a decrease in really
smsll values of
ct
. The reverse - odng
(by several orders of to a more drastic
in formula (21) - can be attained
k
(less
by sim-
than loo9 cm).
increase
only at un-
lie would achieve still
higher values in the ease when the charge should remain constant as the thiclmess of 1, diminishes. um conditions;
therefore,
the lengthy stability
films oannot be attributed Bar
evaluating
expression
nIk, the
(17) for
fI,
where b,
of,
for example, black soap
to that circumstance.
the stabllising
role
of n,
in “8uperthizP
films,
will have to be compared with the expression
molecular component of disjoining
n I
However, this is Incompatible with the equilibrin
for
which is equal to
A
m=q-
Is the effective
pressure,
the
thiclmess
(22)
J of the film,
exceeding
of the same order of magnitude with it 4 . At values
A
h
but being
of the order of
B. V. Derjaguin
360 10-Q
to 10-13,
at L %10-g
and at possible
cm n,
tensides
considered
Of course, order
of
the
of
the structure
adsorbed
ions
their
attraction.
that
the normally
of
“black
it
films”
Our calculations where the surface surface
of
motic
character
of Martinov layers
the behaviour
attention
case,
for
to their
with
the separation
example,
is
is
of
thiclmess
sre
were strongly
a slight trical
permeable
sta-
also,
0
functlthe
in
mobility, neutrality.
the liquid us consider
ion-active,
for
In other
be able
of
the section
in the
SOlUtiOn
interlayer, the case
of
the formation
the contrary
is
to
the Wis-
zones
only
the flow
con-
In view will
over-
solution.
counterions
would infringe
for
that
be separated.
a dense monolayer
of
obvious:
quite of
the
msy be
a pore which,
drop of potential.
the solution
of
osz~sis
of an electrolyte
counterions
the os-
the molecules
the surface
of
not
and inasmuch
The ions
tc purify
osmosisa
The following
bulk.
words,
of “reverse
the capillary
as we have seen,
of
problem
are used,
all
then,
and the flow
the appearance
the membrsne will
there
has attract-
and biological
by how the concentration
across
from that
in the interlayer
would cause
7
interlsyers
we assume to be slit-shaped,
of let
determined
distributed
different
of all,
be present
is
simplicity,
centration
it
C,
in the process
denomination,
but such that
effect
solvedW component
First
dis-
of ionogen
the technical
to be separated. In such membranes, 7 observed rather thsn the ordinary osmosis.
lap.
to
calculations.
case
liquid
mixture
a small
close
to the case,
to the limit
of
the long-time
of diesociatlon
of “ultrathin”
in connection
contrary
membranes,
the sake of
that
applicable
and
has been shown
at very
of developed
as a result
This corresponds
6 it
are attracted
in favour
Muller
_and may even lead
snd Gnilga
speaks
k
character
the diatribution
repulsion
not be underestimated
chsrged
the discrete
of
should
the membrane separation,
In that
of
of
calculations.
Recently, ed a great
is
at the values
to become perceptible.
are simultaneously
groups.
aforementioned
when the effect
dipole
by ion-ac-
interlayers
efficient.
electrostatic
In the study
Nonetheless,
bility
tc be very
begins
their
that even
l
the discrete
oriented
has been found
made become8 incorrect
of monolayer6
decreases
& , it
of
of “ultrathin”
a few monolsyers,
5 have shown that
I%Jaguin
tances.
proves
the calculation
on
onal
n,
>
the mechanism of stabilization
Thus, tive
values
If would
possess
on the elecof counterions Therefore,
from such a0 electrolyte.
but
361
Selected Works - 1
Of course, at high filtration rates the purification degree will drop owing to the fact that the entraining aud the carrying away of counterions will be accompsnied by dosorption of adsorbed ions. sow, let us oonsider the flow of a solution of nonelectrolytes through the membrane. The author snd his ooworkers examined the capillary osmosis of solutioas of nonelectrolytes. The existence of the latter in the light of the theor? developed by the author
7 proves
the
diffuse structure of the mo-
vable psrt of au adsorption lajer. Using this as the basis, the separation effect of reverse osmosis will have to be exsmined; it would be more correct to designate it as "reverse capillary osmo8i8". The factor common to both OffeCtS are the moleculsr forces acting upon the molecules dissolved close to the interface. By snalog~ dth
Lifehits' method for deriving the forces
of paired interaction of molecules, the energy of effective attraction of dissolved molecules of a diluted solution to phase surface8 was established in a study dealing with the theoretical aud experimental investigation of oapillarj 088osis 8,
u (h) = -
A
77
(23)
where
(24) where h. is the distance from the interface, ti is the Plsnck constant, is the solution pemaittivitj,
is
the permittlvity
E,
Is
the permlttivity
of the wall, C is
of the solvent,
f, E3
the number of molecules that are dis-
solved in the solution volume uuit. All &; sre taken as a function of imaginary frequency i 5 . Using Boltzmann~sequation, we find the concentration of dissolved molecules in sn interlayer of thiclmess L
by formula:
(25)
In the
case
if
A
is
ptm~tivo,
we hare t
C>C,’ %!hls,
(26)
as was shown by Churaev g , is conducive to the fact that filtration
of a solution through a membrane is accompaniedby a concentrationdrop of
dissolved molecules, which till just be characteristic of its separation eifect.
6. V. Derjaguin
Another importantcorollary of Bquation (25) consiste in that it groves to be impracticableto apply Dsyaloshinskij,Lifshits snd Pitaevsldjformula to the calculationof the disjoiningpressure of au solution interlayer, the formula supposing the uniformityof the interlsyer.This problem was solved by Churaev and me lo by using Gibbs-D&em's equationwhich allowed the disjoiningpressure of the interlayerof nonelectrolytebinary solution to be expressed by formulat fi
n=-
ar (h) ---d/*-4%, -a
(27)
--bo
where r(k) is the excess number of dissolvedmolecules in the system at a given value of the chemical potential of the solute,p, values of pressure 10 aud temperatureT
and the prescribed
, the number of the molecules of
the solvent and the concentrationof dissolved molecules C,
in the solu-
tion bulk, at a distance of plates L as compared with distance A
Wglo,
flI?designates the disjoiningpressure of an interlsyerof the pure solvent at the same thickness L
The value of /7fi csn be accuratelycslculatedby
Lifshits et al'." formula, if, of course, the structuralpeculiaritiesof the solvent close to interfaceswith plates be disregarded.Rormulas (23), (24), (25) and (27) allow calculating n
.
Analysis of the equations derived has shown the followingr the dispersion component of disjoiningpressure may be positive, if eon&ant
A
is
positive and sufficientlygreat (supposingthat the influence of electromsgnetic retardationis not yet essential).!i!his consequenceof our theory is in
qualitativeagreementwith findings of Sheludko and Rkserova I2 relative
to the stability of free films of butyric acid aqueous solutions.It will be of interest to check the developed theory for the case where both eurfaces are unlike, n,,,=0 , and, hence, fl is completelydeterminedby the overlapping of adsorptionatmospheres.In the studies of Kuuy, Rueanov snd Brodskij I3 , the disjoiningpressure of the interlayersof solutionsis interpretedon the basis of taking into account paired interactionssnd without using formulas (24) and (27) derived by us. !Rhisdoes not allow obtaining quantitativeresults, when using macroscopicconstants as the starting point. At present, there has been accumulateda great amouut of experimental data showing that in a number of cases the consideredoomponentsof disjoining pressure are insufficientfor explaining the interactionof phases separatedby thin interlayers.In particular,the interactionarising changes
Selected Works - 1
363
abruptly with the nature of the eurface a8 a reeult -nonactive
tenaides.
the forth
component of disjoining
are overlapped,
There are relevant
whose etrwture
one under the Influence
of the interface.
proved unambiguouely Therefore, carried
featwee
referring
out reoently pressure.
we shall designate
of tbia component ie
owing to the fact
that the theor
ha8
and due to a emall number of studies,
of the boundary layers
to a number of original
br Ninham et al.14, of the existence
!Ehemost direct
of liquids
in
have been
surfaces
result8
we limit
ourselves
of the struotural
to setting
forth
component of dis-
pressure of wetting filme of water on
of quartt,, glaes,
eented the e%perimentd
studies that have been
and unambiguous proof6 were obtained by
examining the isotherm of disjoining hydrophylic
that
.
the experimental proofs joining
Hereinbelow,
one. The erirtence
insuffioientlj,
whiah the structural
to believe
has been changed a6 oompared with the bulk
but with a great delay,
been developed jet
ground8 available
preeeurs appears when the boundary lwers
that component a8 the structural reoognised
of adsorptionof ion-
mica (muecovite),
In Fig.1 are pre-
of various author6 ‘5s’6*‘7
determining /Tfi)
I 12.
Fig. 1. MejoinIng 1. Water
IO’
0 8.10'
peesure
04.104
isothermal for wetting
on mica I5
fi-films /
2. Rater on glaae I5
3. 2.10-5 N aqueous KC1 solution 4.
5.
IO4 N aqueous NaCl solution Water on quarts 16
on quarts
16
on glaee I5
6. Water on quarts I7
for water on auarts and glase
K-8. These data, like the first measurementa made by Derjaguin and Kueakov 15 , were obtained by resorting to a method of Preeeing a gae bubble to a flat
plate,
and of measuring the equilibrium
9. V. Derjaguin
364
thicknessof a netting
film h and the capillarypressure of the bubble,
which correspond to each other. It is obvious that for great thicknessand, accordingly,small values of /J , the experimentalpoints of different authors are located close to a curve that was plotted according to Langmuir I8 equation !=zE
n,=,-
y2
0 c
_e
.
J
(28)
‘J!his equation defines the ionic-electrostatic componentof the disjoining
pressure of a wetting film in the assumption that the substratepotential is very great (~o>lOO mV), the charge of the free surface is equal to zero, while the (dimensionless)
thickness
Xh
4~.
is
smalls
1.
(29)
However, when fl of the wetting film increases and it accordingly grows thinner, it goes beyond the boundary of stability (or rather metastability). In such a case, there occur local breakups, In which there form thinner sections.Eventually,the greater part of the film acquires a smaller stable thickness,while the remaining part of the initial thicker film breaks up into small lenses forming with the thin film the final contact angle of the ordex of 5 to IO*.
The
branch of the isotherm of disjoining
pressure correspondingto thinner wetting films was obtained in a number of studies I9 , by plotting the dependence of the thicknessof polymolecular "adsorbed"films of water on the relative pressure of vapour p/T, beginning with p/f5=f
, where 'pS is the pressure of vapour over the flat surface of
the same liquid in bulk. pig. 2 representson one graph both
sections/of
the /'7(h)isotherm, i.e. that of thicker,b -layers end that of thinner, h, 200
ii
(a)
Fig. 2. L vs
n drdcm*-isotherm for water on glass, 15, 4- film I9 (curve 1); e isotherm (curve 2); L vs flmisotherm(curve 3).
Selected Works- 1
365
d-layers 20 . The lower part of B -section correspondsto the metastable states of a wetting film. A remarkable fact is that & - section of thinner layers of n(h) isotherm intersects the orinate correspondingto the value n=o
at a finite value
h= k,. The values
a Corollary
of
0
a following
0.
*
dh c
(31)
Owing to this condition, anj variation in thicknesswill increase due to an exchangewith the vapour phase. On the same figure, curve 2 represents isothermwhich has been plotted according to equation (28) that gives & the maximum possible limit of n, values within the range of small thicknesses. Curve 3 represents the dispersion component, fl,, which for ll/-=20of
ConstantA
300 A"
satisfiesequation:
, which was
calculatedby B.V.Churaev20 according to E.M.Lif-
ehits et al.* theor on the basis of quartz end water absorptionspectra, has value A=-
Y, 42 . fo-3
ew.
(33)
Thus, it is obvious that the superimpositionof components fl, and n, of disjoiningpressure is not able to give, even approximately,the Isotherm which was observed within the region of d -layers. Moreover, bj this means it is impossible to explain the reversing of the sign of This is an unambiguousproof that d the
StrUCtUrSl
n(h) at A = L,
- branch of the isotherm stems from
peculiaritiesof water layers that are adjacent to the
quartz surface. This is also substantiatedbr the temperaturedependenceof the characteristicthickness A, of d-
layers. The value of /I., decreases
as temperatureis raised, and at to - 70" it is reduced to the monolayer thiclmess21 . That the observed isotherm of disjoining pressure cannot be ascribed to Van der Waals force8 aleo reeulte from the fact that hjdropho-
366
B. V. Derjaguin
bization cular
of glass
1aJers
explained
with a monolayer
lar
to the disappearance
of water under any pressures
on the basis
of
Now, the isotherms -polar
leads
liquids
of water vapour.
the molecular
of
attraction
the disjoining
on some substrates
component of disjoining
pressure,
as en example the isotherm
of
n,
of wetting
identified
. In Rig.3,
the disjoining
This cannot
be
#laws.
pressure
may be fully
of poljmole-
with
there
pressure
films
of non-
the molecu-
is represented
of h -hexane
wetting
- h,ii
(b)
’ 600
- 400
.
I
.
,
400 Fig.
film
3.
n
200 vs
d&cm2
22 . Measurements
on steel
thickness
instead
to plotting
isotherm:
with
6
the film,
limit
case
of water, change
of
distances
= -1.6.10
the full
effect
would be natural
the substrate.
of
of
scores
disturbs
tural
of disjoining
component
structural
the assumption component,
Examination ther
substantiation
of
having
a formula
thickness was applied
(34)
of
and corresponds
erg. cm
electromagnetic
to ascribe
the order kgstrdm.
the s~sten
of for
the structural
of
architecture correlation
disappear influence
is able
the viscosity
of
of
peculiarities.
structural
bonds;
peculiarities
thin
only
layers
of
to a
active
csn be restored
at
length,
which is
higher
than 70%,
therefore,
, too. of
in the
23 . In case
bonds under the effect
of hydrogen
the possible solubility
retardation
At temperatures
pressures
to the interaction
the hind of metal used,
from
Such a disturbed
the heat motion
refutes
-19
of hydrogen
from the surface
on the order
(32),
on steel.
A4
in the architecture
centers
water
it
films
to the films
of formulas
which is independent
of
R-hexane
-0 =-,
“* where constant
of
were limited
more than 400 ii. Therefore, the theoretical
I,“”
.
also
solubility
to grow with of water
the struc-
This fact
quarts
on the
temperature.
serves
An increased
for
as a fur-
ViSCO8itJ
of
367
Selected Works- 1
those layers on the quartz-glassinterfacewas detected on observingwhether the flow of rater in quartz capillaries24 up to 200 i in radius, or the flow of thin water films wetting glass and quartz 25 . In layers about 50 i thick, at a temperatureof about 20°C there is observed an increase in
ViS-
cosity by several times as compared with the bulk value. It is remarkable that this increase in viscosity disappearsat the same temperatureof 70°C, at which the structuralcomponent of disjoiningpressure disappears. Finally, the structuralpeculiaritiesof boundary layers of water were independentlyproved by examining thermoosmosiswhich was detected in 1947. This phenomenonconsists in the flow of liquid through glass capillariesor 26 . In accordance diaphragmpores under the effect of a temperaturegradient with Derjaguin'stheory 26 based on using thermodynamicsof irreversible processes, the thermoosmoticflow rate
through a capillaryhaving the dt form of a slit with thickness h is equal to:
(35) where
h/z d //(x)x(h-xld3: X"
J
"J)
9
(36) 0 where a/f is the excess of the enthalpy density as compared with the bulk is viscosity,X is the coordinatewhich is read off one surface of value 9‘3 the slit. It is supposed that the width of the capillary is much greater than the width of leyers in which the specific enthalpy is different from the bulk value. Part of the change in the enthalpy may be ascribed to the effect of ionic atmospheresthat form close to the slit surfaces.For water, this part is small, as follows, firstly, from an insignificantinfluence of the electrolyte concentration,and secondly,from the fact that thermoosmosisintensity which decreases as temperatureincreases,disappears at a temperature of 7ow 27 . Peculiar is the dependenceof the thermoosmoticflow on the capillary radius (see Fig.4). At great radii (on the order of 1 ,um>, the thermcosmoticflow is directed towards the increasing temperature,and its flow rate is comparativelysmall. As the capillary radius (see Pig.4) decreases below 500 1, the direction of the .thermoosmotic flow changes to the directly opposite one, i.e. in the direction of decreasing temperature,and, what is the most
surprising,
it
increaseswith a further decrease in the ra-
dius. The change in the direction of thermooamosisto the directly opposite
368
B. V. Derjaguin L_
__I_.._
10
100x -_
100
1%
I~
1
t=200c
! !
I.grad T=200”cm-I 2gradT=250°cm-1
2
2 I 01 -2L-L
I
1
_.__-.
_-
5
10 Lni
Fig.
4.
Thermoosmosis
one with
the layer
of water
consists
and for
fluence
of
one another
Zt
flow 15
ctional
appearance face
(for
bodies
component
mentioned
the change
-ionogen
surfactants
example,
polyglycol
adsorption.
study
an adjacent
pressure
centers
or radii
layers
overlap
hydrosol
layers.
of
of
there able
iodide
additions
of
is
chains
the
the sur-
of
appears
the
to guarantee
silver
the valence
fun-
can be modified
there into
the
may be lyophilic
concentrated
so-
the counterion).
achieved
medium, the surfactants
oxaethyl
active
Hence,
As an example, of
of
that determines
which is
2g that modification
having
h
in the thermo-
phase,
particles)
system.
to the aqueous
the in-
such a change in
an increase
As a result,
under the effect
esters
Without
colloid
colloid
capillaries,
un-
themselves. of
lyophobic
(independently
to Glazman’s
to explain
is positive,
thicknesses
them changes.
layer
to indicate
as the boundary
(or
of lyophobic
of electrolytes
for
narrow
of disjoining
only
of
of boundary
a corresponding
coagulates
radii
peculiarities
of monolayer
of
According
each of
impossible
at smaller
OH) and charged
example,
stability
lutions
prevails;
on the surface
structural
under the effect
one that
of
whereas
the boundary
one of which AH
is
h or
would be impossible
of lyophobic
structural
layer
for it
thicknesses
Is greater,
the presence
of
that
two layers,
as the capillaries
groups
unambiguously
negative
another
it
raaaus.
of
the structure
the structure,
proves
capillary
28 . However,
one layer of
vs
at least
why at greater
the influence
osmotic
thickness
the other
ambiguously
rate
of different
by adding being,
for
lengths.
non
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